Water Resources Division, U.S. Geological Survey
1943, Water Supply Paper 925
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Publication Extents
Not all publications have extents, not all extents are completely accurateWater Resources Division, U.S. Geological Survey
1943, Water Supply Paper 928
Th!s volume is one of a series of 14 reports presenting results or measurements of stage and flow made on streams, lakes, and reservoirs in the United States during the water year ending September 30, 1941. The work was begun !n 1888 in connection with special studies relating to irrigation....
Water Resources Division, U.S. Geological Survey
1943, Water Supply Paper 924
Walter S. White, John H. Eric, Thomas William Amsden
1943, Open-File Report 79-352
No abstract available....
J.F. Smith Jr. , L.L. Ray
1943, Geological Society of America Bulletin (54) 891-924
In north-central New Mexico the rugged Cimarron Range marks the eastern margin of the Southern Rocky Mountains, abruptly rising more than 5000 feet above the adjacent Great Plains. Structurally the range is a northward-plunging anticline with a core of pre-Cambrian crystalline rocks. Faulting along the eastern and western margins of...
Hugh Dinsmore Miser
1943, Economic Geology (38) 91-118
An important chapter of the total geologic history of the Ouachita Mountains is revealed by the quartz veins and crystals. These and the associated minerals are hydrothermal deposits of probable magmatic origin, formed during the closing stage of the mid-Permsylvanian orogeny. The metalliferous deposits of the Ouachita Mountains appear to...
Lyman C. Huff
1943, Eos, Transactions, American Geophysical Union (24) 573-580
Water‐levels in wells, which are utilized by the hydrologist as a measure of ground‐water storage, customarily are measured in terms of distance below a convenient measuring point and expressed with reference to a fixed datum. Datum‐planes or surfaces of several types have been used—each serving some particular purpose advantageously. These...
C. E. Jacob
1943, Eos, Transactions, American Geophysical Union (24) 564-573
Long Island simulates in a general way an aquifer in the form of an infinite strip confined between parallel boundaries at constant head (sea‐level), over which recharge precipitation is assumedly uniform. The non‐steady flow of water in this idealized system is analyzed assuming provisionally that the effective thickness of saturated...
John T. Hack
1943, American Antiquity (8) 235-241
This report is based on two months reconnaissance in the summer of 1941 in the Eden Valley, Wyoming. The work is as yet far from complete and the conclusions presented here must be regarded as tentative. It is hoped that in the future more extensive geological work may be undertaken.The...
Walter B. Lang
1943, Science (98) 173-174
No abstract available....
Leland K. Wenzel, A.L. Greenlee
1943, Eos, Transactions, American Geophysical Union (24) 547-564
Ground‐water has long been recognized as one of our important natural resources, but only in about the last 20 years has concentrated effort been made to place ground‐water hydrology on a quantitative basis. The quantitative approach to ground‐water work has been brought about largely through the leadership of O. E....
Jewell J. Glass
1943, Eos, Transactions, American Geophysical Union (24) 252-257
The recent discovery of the widespread occurrence of helvite, a beryllium‐bearing mineral, at Iron Mountain, New Mexico, has aroused interest in the commercial possibilities of a mineral which heretofore has been considered to have only scientific significance. Helvite contains about 13 per cent beryllium oxide as compared with five to...
W. G. Hoyt, Bertram Barnes, H.L. Cook, E.S. Cullings, G.A. Hathaway, Karl R. Jetter, N.H. Leupold, Phillip Light, C. C. McDonald, F.T. Mavis, L.K. Sherman, Waldo E. Smith, F. Snyder, H.G. Wilm
1943, Eos, Transactions, American Geophysical Union (24) 422-423
The Committee on Runoff was not formally constituted until February 6, 1943, when the members of the Section, as listed above, were asked to serve. At the suggestion of President CHURCH the Committee has been so selected that there is Nation‐wide geographic distribution from West to East with the majority...
O. E. Meinzer
1943, Article
The very large service which the geologists and engineers trained in ground‐water hydrology are rendering in this country in the prosecution of the war is due largely to the effective organization for this purpose. The Federal agency in which this service centers is the Water Resources Branch of the United...
Francois E. Matthes
1943, Eos, Transactions, American Geophysical Union (244) 389-401
The personnel of the Committee at present is as follows:Harry Fielding Reid, Professor Emeritus of Geology, Johns Hopkins University, 608 Cathedral Street, Baltimore, MarylandWilliam H. Hobbs, Professor Emeritus of Geology, University of Michigan, Ann Arbor, Michigan Colonel Lawrence Martin, Chief, Division of Maps, Library of Congress, Washington, D.C.James E. Church,...
George C. Kennedy
1943, Eos, Transactions, American Geophysical Union (24) 257-257
Some of the large, low‐grade nickel‐copper deposits of Bohemia Basin, Yakobi Island, south‐eastern Alaska, which previously had been mapped and studied by the United States Geological Survey, were explored during parts of 1941 and 1942 by the United States Bureau of Mines. The Gealogical Survey interpreted the geologic features of...
N.A. Rose
1943, Eos, Transactions, American Geophysical Union (24) 420-421
In view of the shortness of time since the appointment of the writer to the Committee on Ground Water this report is confined to the technology and problems in the Gulf Coast Oil Province. Of course, many of the methods and practices would apply to most parts of the country...
Robert E. Fellows
1943, Eos, Transactions, American Geophysical Union (24) 271-271
The lower limit of visible traces of penetrative movement in quartz‐rich rocks can be defined by studies of orientations and mutual relations of grains. Intensity of deformation in the central Appalachians decreases gradually from the crystalline Piedmont toward the north, northwest, and west perpendicular to the regional trend. The author...
O. E. Meinzer
1943, Eos, Transactions, American Geophysical Union (24) 418-418
No abstract available. ...
Joseph E. Upson
1943, Report
The Lompoc Plain is the central lowland of a topographic and structural basin that forms the western and lower part of the Santa Ynes Valley in Santa Barbara County, California. It extends inland about 11 miles from the coast and is 1 mile fto about 3 miles wide....
U.S. Fish and Wildlife Service
1943, Wildlife Leaflet 240
No abstract available....
U.S. Fish and Wildlife Service
1943, Wildlife Leaflet 239
No abstract available....
John Beaver Mertie
1943, Economic Geology (38) 298-312
Several problems may arise in the geometrical determinations of strike and dip from core drilling. If the stratigraphic or structural surfaces are plane, as the bedding planes of a homocline, two problems may exist, depending upon whether the drill cores do or do not penetrate to some recognizable horizon. The...
Stanley G. Jewett
1943, Wildlife Leaflet 238
No abstract available....
Branch of Predator and Rodent Control U.S. Fish and Wildlife Service
1943, Wildlife Leaflet 237
No abstract available....